The significance of a geochemically isolated intracrystalline organic fraction within biominerals

Gerald A. Sykes, Matthew J. Collins*, Derek I. Walton

*Corresponding author af dette arbejde
    113 Citationer (Scopus)

    Abstract

    In studies of organic matter in fossil biominerals, there has been a widespread failure to distinguish between the organic matrix and organic matter trapped within the crystal elements. The existence of chemically isolated (intracrystalline) proteins are indicated by the persistence of amino acids after prolonged treatment with a strong chemical oxidant (NaOCl). The geochemical significance of these residual amino acids is illustrated by the re-analysis of aberrantly young d-aile/l-ile ratios (0.142 ± 0.042, n = 4) of amino acids from a land snail (Cepaea sp.) collected from Tattershall Thorpe in Lincolnshire. Following NaOCl treatment the d-aile/l-ile ratio increased (0.178 ± 0.014, n = 5), while both the total amino acid concentration and the variance declined.

    OriginalsprogEngelsk
    TidsskriftOrganic Geochemistry
    Vol/bind23
    Udgave nummer11-12
    Sider (fra-til)1059-1065
    Antal sider7
    ISSN0146-6380
    DOI
    StatusUdgivet - 1 jan. 1995

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